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A nanopetrographic and textural study of grain-coating chlorites in sandstone reservoirs

Published online by Cambridge University Press:  09 July 2018

V. Billault ,
D. Beaufort ,
A. Baronnet  and
J. -C. Lacharpagne
V. Billault*
Affiliation:
Laboratoire Hydr'ASA, CNRS-UMR 6532, 40 avenue du Recteur Pineau, 86022 Poitiers, France
D. Beaufort
Affiliation:
Laboratoire Hydr'ASA, CNRS-UMR 6532, 40 avenue du Recteur Pineau, 86022 Poitiers, France
A. Baronnet
Affiliation:
Centre de Recherche sur les Mécanismes de la Croissance Cristalline, CNRS-UPR 7251, Campus Luminy, Case 913, 13288 Marseille Cedex 9, France
J. -C. Lacharpagne
Affiliation:
TOTALFINAELF, Avenue Larribau, 64018 Pau, France
*
*E-mail: valerie.billault@hydrasa.univ-poitiers.fr
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Abstract

Scanning electronic microscopy (SEM) and transmission electronic microscopy (TEM) investigations of chlorite grain coatings from four different sandstone reservoirs indicate a progressive change in both texture and arrangement of chlorite particles from the contact with the detrital substratum to the centre of the pore. Such spatial distribution results from growth by geometrical selection. Geometrical selection of chlorite crystals proceeded during a single event of continuous growth which began before the consolidation of the sandy sediments, lasted through part of the subsequent mechanical compaction and ceased before the occurrence of quartz cement. Nanopetrographic investigations near the detrital quartz-chlorite coating interface demonstrate that inhibition of the quartz cement is due to the limitation of the epitaxial growth of quartz to the interparticular space at the base of the chlorite coating and not an absence of nucleation. It is suggested that these results can be applied to most of the sandstones which contain Fe-rich chlorite grain coatings.

Keywords

clayschloritesandstoneTEMSEMAEMburialdiagenesis
Type
Research Article
Information
Clay Minerals , Volume 38 , Issue 3 , September 2003 , pp. 315 - 328
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 2003

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References

Billault, V. (2002) Texture, structure et proprié tés cristallochimiques des chlorites ferreuses dans les réservoirs gréseux. PhD thesis, Univ. Poitiers, France.Google Scholar
Bjorlykke, K., Nedkvitne, T., Ramm, M. & Saigal, G.C. (1992) Diagenetic processes in the Brent Group (Middle Jurassic) reservoirs of the North Sea – an overview. Pp. 263–288 in: Geology of the Brent Group(Morton, A.C., Haszeldine, R.S, Giles, M.R. & Brown, S., editors). Geological Society of London Special Publication 61.Google Scholar
Dixon, S.A., Summers, D.M. & Surdam, R.C. (1989) Diagenesis and preservation of porosity in Norphlet Formation (Upper Jurassic), Southern Alabama. American Association of Petroleum Geologists Bulletin, 73, 707–728.Google Scholar
Dutton, S.P. (1977) Diagenesis and porosity distribution in deltaic sandstone, Strawn series (Pennsylvanian), north-central Texas. Gulf Coast Association of Geological Societies Transactions, 27, 272–277.Google Scholar
Ehrenberg, S.N. (1990) Relationship between diagenesis and reservoir quality in sandstones of the Garn formation, Haltenbanken, mid-Norwegian continental shelf. American Association of Petroleum Geologists Bulletin, 74, 1538–1558.Google Scholar
Ehrenberg, S.N. (1993) Preservation of anomalously high porosity in deep buried sandstones by grain- coating chlorite: Example from the Norwegian Continental Shelf. American Association of Petroleum Geologists Bulletin, 77, 1260–1286.Google Scholar
Girard, J.P., Munz, I.A., Johansen, H., Hill, S. & Canham, A. (2001) Conditions and timing of quartz cementation in Brent reservoirs, Hild Field, North Sea: constraints from fluid inclusions and SIMS oxygen isotope microanalysis. Chemical Geology, 176, 73–92.Google Scholar
Grigor’ev, D.P. (1965) Ontogeny of Minerals. Israel program for scientific translations Ltd, Marson, S., Jerusalem.Google Scholar
Grigsby, J.D. (2001) Origin and growth mechanism of authigenic chlorite in sandstones of the lower Vicksburg formation, South Texas. Journal of Sedimentary Research, 71, 27–36.Google Scholar
Hayes, J.B. (1970) Polytypism of chlorite in sedimentary rocks. Clays and Clay Minerals, 18, 285–306.Google Scholar
Heald, M.T. & Larese, R.E. (1974) Influence of coatings on quartz cementation. Journal of Sedimentary Petrology, 44, 1269–1274.Google Scholar
Hillier, S. (1994) Pore-lining chlorites in siliciclastic reservoir sandstones: electron microprobe, SEM and XRD data, and implications for their origin. Clay Minerals, 29, 665–679.Google Scholar
Hogg, A.J.C., Pearson, M.J., Fallick, A.E. & Hamilton, P.J. (1995) An integrated thermal and isotopic study of the diagenesis of the Brent Group, Alwyn South, U.K., North Sea. Applied Geochemi stry, 10, 531–546.Google Scholar
Imam, M.B. (1986) Scanning electron microscopy study of the quartz overgrowths within Neogene sandstones of Bengal Basin, Bangladesh. Journal of Geological Society of India, 28, 407–413.Google Scholar
Jahren, J.S. (1991) Evidence of Ostwald Ripening related recrystallization of diagenetic chlorites from reservoir rocks offshore Norway. Clay Minerals, 26, 169–178.CrossRefGoogle Scholar
Land, L.S., Milliken, K.L. & McBride, E.F. (1987) Diagenetic evolution of Cenozoic sandstones, Gulf of Mexico sedimentary basin. Sedimentary Geology, 50, 195–225.CrossRefGoogle Scholar
Larese, R.E., Pittman, E.D. & Heald, M.T. (1984) Effects of diagenesis on porosity development, Tuscaloosa sandstones, Louisiana (abs). American Association of Petroleum Geologists Bulletin, 68, 498.Google Scholar
Odin, G.S. (1988) Green Marine Clays, pp. 5–52. Elsevier, Oxford, UK.Google Scholar
Pittman, E.D. & Lumsden, D.N. (1968) Relationship between chlorite coatings on quartz grains and porosity, Spiro Sand, Oklahoma. Journal of Sedimentary Petrology, 38, 668–670.CrossRefGoogle Scholar
Robinson, A. & Gluyas, J. (1992) Duration of quartz cementation in sandston es, North Sea and Haltenbanken Basins. Marine Petrology and Geology, 9, 324–327.CrossRefGoogle Scholar
Ryan, P.C. & Reynolds Jr, R.C. (1996) The origin and diagenesis of grain-coating serpentine-chlorite in Tuscaloosa Formation sandstone, U.S. Gulf Coast. The American Mineralogist, 81, 213–225.CrossRefGoogle Scholar
Thomson, A. (1979) Preservation of porosity in the deep Woodbine/Tuscaloosa trend, Louisiana. Gulf Coast Association of Geological Societies Transactions, 30, 396–403.Google Scholar
Tillman, R.W. & Almon, W.R. (1979) Diagenesis of the Frontier formation offshor e bar sandstones, Spearhead Ranch field, Wyoming. Section of Economic Paleontol ogists and Mineralog ists Special Publication, 26, 337–378.Google Scholar
Walderhaug, O. (1994) Temperatures of quartz cementation in Jurassic sandstones from the Norwegian continental shelf: evidence from fluid inclusions. Journal of Sedimentary Research, A64, 311–323.Google Scholar